not quite significantp -value = 0.097
Iron levels in the Fe HH phase in basaltic tephra and sediment were not quite significantly different ( p -value = 0.097) but lower in the basalts.
Iron levels in the Fe HH phase in basaltic tephra and sediment were not quite significantly different ( p -value = 0.097) but lower in the basalts.
The Fe total in sediment and in andesitic or trachydacitic tephra were significantly not different ( p -value = 0.158) ( Table 2 ).